Find Concrete Repair Contractors in Hillsborough, NH

If you need concrete leveling in Hillsborough, the usual culprits are dense glacial-till mantle with Hollis, Charlton, Paxton, and Woodbridge till-derived sandy loams and fragipans, and frost-susceptible silt-rich till producing aggressive freeze-thaw heave. Hillsborough is a town in northwestern Hillsborough County, southwestern New Hampshire, sitting along NH-9, NH-31, NH-149, and US-202 about 25 miles west of Concord and 25 miles north of Peterborough. In 1735 and 1736, Colonel John Hill was granted a tract of land about six miles square and named it Hillsborough (with the "s" being added later). He started a community with a generous tract of land, which would be known as Hillsborough Center. Benjamin Pierce came to Hillsborough to survey land and was so taken by the town that he bought a small cabin and farm and settled, becoming involved in local and state politics and serving twice as Governor of New Hampshire; Benjamin Pierce assembled an estate of several hundred acres between 1785 and his death in 1839. The Franklin Pierce Homestead, the childhood home of the 14th president of the United States Franklin Pierce, was built in 1804 (with the main block) and is now a historic house museum and state park; the home remained in the Pierce family until 1925, when it was donated to the state of New Hampshire, and was declared a National Historic Landmark in 1961. In the 1840s, the decline in farming was met with the rise of the industrial era in New Hampshire: some farmers moved to more fertile lands of the Midwest, but others found work in the new mills rising along the Contoocook River, and at this time the Upper and Lower Villages and the Center Village became overshadowed by the booming Hillsborough Bridge village where a half dozen mills used energy from the Contoocook. Today Hillsborough (population 6,196 at the 2020 census) is the regional service center for the western Contoocook Valley with significant historic and post-industrial character. Hillsborough sits on the rolling till-mantled bedrock terrain of southwestern New Hampshire, in the Contoocook River drainage tributary to the Merrimack. Bedrock is principally Devonian Concord-type granite plutonic intrusions of the New Hampshire Plutonic Suite, with Devonian Littleton Formation schist and quartzite of the Central Maine Belt locally. Above bedrock, late Wisconsinan glacial till (a stony sandy loam mantle deposited 14,000 years ago by the retreating Laurentide Ice Sheet) blankets the hillsides, with glaciofluvial outwash (sand and gravel) along the Contoocook corridor, glacial-lake-deposited fine sediments in some valley bottoms, Holocene Contoocook alluvium and organic peat in wetlands, and historic mill-tailings-and-fill on the Hillsborough Bridge mill-village industrial-corridor parcels. Local soils include Hollis and Charlton complex on the till uplands (the dominant southern New England forest soil; Hollis is shallow-to-bedrock and Charlton is deeper till), Paxton fine sandy loam on the till uplands (with significant fragipan), Woodbridge fine sandy loam on the till uplands (poorly drained over fragipan), Ridgebury fine sandy loam on the till lowlands (very poorly drained), Hinckley loamy sand on the outwash terraces (excessively drained kame-and-esker glaciofluvial), Windsor loamy sand on the outwash sand plains, Searsport mucky peat on the wetland flats, Saco silt loam on the alluvial flats, and gravelly alluvium along the Contoocook corridor. Between dense glacial-till mantle with Hollis, Charlton, Paxton, and Woodbridge till-derived sandy loams and fragipans, frost-susceptible silt-rich till producing aggressive freeze-thaw heave, perched-water cycling on Paxton and Woodbridge fragipan parcels driving subgrade saturation, granite shallow-bedrock differential bearing on bedrock-near-surface parcels, glacial erratics producing localized hard spots, the historic Hillsborough Center and Hillsborough Bridge mill-village industrial-corridor parcels with century-and-a-half-old foundations and mill-tailings-and-fill backfill variability, the Franklin Pierce Homestead National Historic Landmark coordination flatwork, and steady Contoocook-Valley regional-service-center commuter and rural residential cut-and-fill on the dispersed parcels, subgrade behavior is the primary driver of slab movement here.